The monitoring network within this area

Hydrionis holds 1,065 values from 6 gauges within it. Discharge is a property of a gauge and its reach, not of this drainage area, so this page reports the network and its records rather than a single figure.

6
Gauges
1,065
Values held
1919–2026
Record spans
Gauges within the Upper Neuse huc8 subbasin
6 monitoring points, positioned as the publisher records them.
Gauges within the Upper Neuse huc8 subbasinENO RIVER AT HILLSBOROUGH, NC, FLAT RIVER AT BAHAMA, NC, FLAT RIVER AT DAM NEAR BAHAMA, NC, NEUSE RIVER NEAR NORTHSIDE, NC, DIAL CREEK NEAR BAHAMA, NC, NEUSE RIVER NEAR CLAYTON, NCENO RIVER AT HILLSBOROUGH, NCFLAT RIVER AT BAHAMA, NCFLAT RIVER AT DAM NEAR BAHAMA, NCNEUSE RIVER NEAR NORTHSIDE, NCDIAL CREEK NEAR BAHAMA, NCNEUSE RIVER NEAR CLAYTON, NC

Flood peaks, as measured

This gauge's flood record, as measured. Unlike a daily mean it is the discharge at the moment the river was highest, which is the figure flood frequency analysis is built on.

Largest measured flow of each year at FLAT RIVER AT BAHAMA, NC
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1926–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at FLAT RIVER AT BAHAMA, NCLargest measured flow of each year at FLAT RIVER AT BAHAMA, NC: FLAT RIVER AT BAHAMA, NC in m³/s, from 1926 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s19261939195219651976198920002013

Published by the gauge's own operator from its sub-daily record; Hydrionis stores the figure rather than recomputing it. A year the gauge did not cover produces no value rather than a low one, and the gaps are stated below the chart. A peak is a property of this gauge and its reach: a larger flood upstream or downstream of it is not in this series.

What the shaded periods are (1 event)

A shaded period marks when something was recorded, not what caused the shape of the line. Where the two coincide, they coincided.

Documented record — A documented event, compiled from cited sources after it happened. The dates are as good as the record, which for older events can mean the month rather than the day.

EventTypePeriodStandingAuthority
Hurricane Katrina water and sanitation collapseFlood2005-08-29 – 2005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • The 2022 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cantareira water crisis, São Paulo — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cape Town Day Zero — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
View the data behind this chart
Underlying data
PeriodFLAT RIVER AT BAHAMA, NC (m³/s)
1926102
1928246
1929207
1931195
1932201
1933135
1934385
1936246
1937267
1938566
1939260
1940274
1942125
1944226
1945456
1946161
194786.4
1948193
195090.6
1951101
1952297
1954139
1955433
1957190
1958153
1960153
1961122
1962241
1963218
196494.3
1965205
1966167
1967272
1968144
1969137
1970328
197195.7
1973297
1974379
1975493
197660.6
197743.3
1978326
1979205
1981137
1982204
1983297
1984219
198593.4
1987303
1989190
1991169
1992215
1993402
1994202
1995178
1996957
1997145
1998473
1999289
2000174
2001186
200230.6
2004167
200598.0
2006166
2008416
2010209
201163.4
201295.1
2013104
2014289
201582.1
2016388
2018413
2020229
2022100
2023125
2024286
2025532

About this series

Everything below is a property of the data rather than a rating of it. There is deliberately no single confidence score: how much a gap matters depends on what you are about to do with the series, and only you know that.

Source
United States Geological Survey — National Water Information System · US Government work — public domain
How the values came to existMeasured
Period held1926–2025
Completeness80.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 20 separate periods inside 1926–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1926 and is not continuous from it: 100 years separate the first value from the last, and 80% of the years between them are held. The span is not the record.
Last read from the publisher2026-10-01
RedistributionPermitted by the upstream licences
Commercial reusePermitted by the upstream licences. No Hydrionis access tier can widen this.
MethodologyHow this was produced

How much of the rain came back out

A discharge in cubic metres per second cannot be compared with anything: the larger number may only mean the larger catchment. Divided by the area draining to the gauge it becomes a depth of water over that land, which answers a question a reader already has — of the rain that fell here, how much came back out as river?

Water leaving the catchment above FLAT RIVER AT BAHAMA, NC, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1926–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above FLAT RIVER AT BAHAMA, NC, as a depthWater leaving the catchment above FLAT RIVER AT BAHAMA, NC, as a depth: FLAT RIVER AT BAHAMA, NC in mm, from 1926 to 2025.Hurricane Katrina water and sanitation collapse0200400600800mm19261939195219651978199120042018

Computed by Hydrionis from the published annual mean flow and the catchment area the station's own publisher states. It is not a water balance: the difference between rainfall and runoff is not evaporation alone but also change in groundwater storage, water abstracted and taken elsewhere, and water imported by transfer schemes — which is why a catchment can yield more runoff than the rain that fell on it without anything being measured wrongly. A different area figure rescales every value here by the ratio between them.

What the shaded periods are (1 event)

A shaded period marks when something was recorded, not what caused the shape of the line. Where the two coincide, they coincided.

Documented record — A documented event, compiled from cited sources after it happened. The dates are as good as the record, which for older events can mean the month rather than the day.

EventTypePeriodStandingAuthority
Hurricane Katrina water and sanitation collapseFlood2005-08-29 – 2005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • The 2022 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cantareira water crisis, São Paulo — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cape Town Day Zero — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
View the data behind this chart
Underlying data
PeriodFLAT RIVER AT BAHAMA, NC (mm)
1926216
1927262
1928334
1929486
1930187
1931268
1932330
1933203
1934451
1935341
1936552
1937457
1938448
1939443
1940365
1941126
1942297
1943236
1944438
1945469
1946230
1947267
1948502
1949308
1950205
1951204
1952480
1953318
1954213
1955355
1956258
1957302
1958368
1959348
1960437
1961361
1962503
1963251
1964267
1965248
1966189
1967163
1968184
1969231
1970214
1971472
1972463
1973482
1974383
1975632
1976145
1977140
1978494
1979496
1980236
1981155
1982436
1983464
1984472
1985298
1986154
1987368
1988152
1989522
1990340
1991208
1992241
1993447
1994255
1995342
1996541
1997305
1998562
1999343
2000276
2001176
2002243
2003690
2004263
2005211
2006203
2007157
2008238
2009380
2010239
2011111
2012110
2013289
2014351
2015369
2017279
2018600
2019466
2020578
2021319
2022193
2023215
2024437
2025324

About this series

Everything below is a property of the data rather than a rating of it. There is deliberately no single confidence score: how much a gap matters depends on what you are about to do with the series, and only you know that.

Source
United States Geological Survey — National Water Information System · US Government work — public domain
How the values came to existDerived Computed by Hydrionis
Period held1926–2025
Completeness99.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1926–2025 holds no value: 2016. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1926 and is not continuous from it: 100 years separate the first value from the last, and 99% of the years between them are held. The span is not the record.
Inputs last read2026-10-01 · when the records this was computed from were last read from their publishers
Calculation date2026-08-24 · when the calculation method was last versioned, not a reading of any publisher
RedistributionPermitted by the upstream licences
Commercial reusePermitted by the upstream licences. No Hydrionis access tier can widen this.
MethodologyHow this was produced

Every gauge Hydrionis holds within this area

Gauges within the Upper Neuse and what each holds
GaugeMeasuresValuesRecord
FLAT RIVER AT BAHAMA, NCcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2991925–2026
ENO RIVER AT HILLSBOROUGH, NCcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2511927–2026
FLAT RIVER AT DAM NEAR BAHAMA, NCcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2071927–2026
NEUSE RIVER NEAR NORTHSIDE, NCcatchment area, annual maximum river flow, mean river flow, mean river flow, water year1591927–2026
NEUSE RIVER NEAR CLAYTON, NCcatchment area, annual maximum river flow1001919–2026
DIAL CREEK NEAR BAHAMA, NCcatchment area, annual maximum river flow491926–2026

How these gauges were attached to this water

Assigned by the publisher to a numbered basin Every gauge here is assigned to this drainage area by its own publisher, which issues the area an official code — 03020201. A drainage area is not a river: it contains the tributaries as well as the main channel, and a gauge in it may be on any of them.

What each gauge’s link to this water rests on
GaugeEvidenceEstablished
FLAT RIVER AT BAHAMA, NCStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
ENO RIVER AT HILLSBOROUGH, NCStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
FLAT RIVER AT DAM NEAR BAHAMA, NCStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
NEUSE RIVER NEAR NORTHSIDE, NCStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
NEUSE RIVER NEAR CLAYTON, NCStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
DIAL CREEK NEAR BAHAMA, NCStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02

What this record holds

Hydrionis decides which waters get a page, and which of those are offered to search, from what is actually held rather than from how the page reads. Five signals are counted; this record has 4 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record5yes, 3 or more
Years spanned108yes, 20 or more
Values held1,065yes, 1000 or more
Distinct measurements4yes, 2 or more
Publishers measuring it1no
Official identifiers1recorded, not counted

Use this data

Use this data

No bulk download is offered here, which is a licence position rather than a product one: at least one contributing publisher does not permit redistribution. The values can be read on the page, cited, and pointed to at source.

Attribution and citation

Suggested citation for Hydrionis

Hydrionis (2026), Upper Neuse gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-neuse/

Cite Hydrionis where you rely on values Hydrionis computed, on the method that produced them, or on the compilation itself. The underlying measurements remain the publishers’ and their attribution requirements apply to you directly.

Recommended, not required. Hydrionis does not claim rights over unmodified public data it relayed, and doing arithmetic on somebody else’s measurements does not make them Hydrionis’s. Cite the version and the access date: the Upper Neuse gauge records changes as publishers release and as methods are revised, and a citation without both cannot be checked later. Full guidance is on cite and reuse.

None of the contributing licences requires attribution. Crediting the publishers is still good practice and they are listed above.

Where these figures come from

MeasuredHigh confidence2025-07-07

Source: USGS — National Water Information System, USGS site 02085500, annual peak streamflow. Licence: Open.

Method: The instantaneous maximum discharge of each water year as published by USGS, dated to the day it occurred. One value per October-to-September water year; where the publisher lists both a systematic and a historic peak for a year, the larger is the annual maximum. Values the publisher marks as maximum daily averages are not held here, because they are not instantaneous peaks. Values marked as bounded rather than measured are held as censored observations carrying the bound. Cubic feet per second are converted to cubic metres per second and the publisher unit is recorded alongside.

Rating curves are extrapolated at extreme discharges, so the largest values in a peak series carry the largest measurement uncertainty. Data from the U.S. Geological Survey National Water Information System, a work of the United States government and therefore in the public domain.

Retrieved 1 October 2026.